Introduction:
The sea surface temperature field in the eastern tropical
Pacific, with its strong asymmetry about the equator, annual and
interannual variability, and links to climate are of great
interest to the NOAA Pan American Climate Study (PACS) Program.
There is much recent speculation that the tropical Pacific SST
distribution has plays a crucial role in past as well as present
and future global climate anomalies. The sea surface temperature
field is believed to control the strength and location of the
Inter-Tropical Convergence Zone (ITCZ); and this variability in
the ITCZ may in turn influence the location of the jet stream and
precipitation over North America. The ITCZ and the warm water
north of the equator both move north and south annually, but the
details of the coupling between the two are unknown. Our
understanding of the processes that control sea surface
temperature in this region is lacking and uncertainties in
existing climatologies of the surface heat flux, wind stress, and
precipitation are large. The overall goal of the PACS program is
to improve the skill of operational seasonal-to-interannual
climate prediction over the Americas. Thus an improved
understanding of the of air-sea interaction in this region will
likely lead to improvement of forecast skill.
A pilot field study in the eastern tropical
Pacific was conducted as part of a larger, cooperative effort to
investigate air-sea coupling in the tropical regions of the
Americas and its links to climate variability in the Americas. The
observational program began in April 1997 when two surface
moorings were deployed at the 3° S (cold tongue) and 10° N (ITCZ)
on 125° W. Each mooring carried two complete sets of
meteorological sensors (wind velocity, air and sea temperature,
incoming short-wave radiation and incoming long-wave radiation,
humidity, barometric pressure, precipitation, surface currents)
using redundancy to ensure that a complete time series of all
variables will be collected, thus permitting calculation of the
heat, mass, and momentum fluxes via the bulk formulae. The
moorings also carried oceanographic sensors (temperature,
conductivity and current) placed in the top ~150m of the ocean to
monitor the upper ocean variability. The two moorings were
recovered in September 1998. This project covers the scientific
analysis and publication of the mooring data that were collected.
The focus of this study will be on sea surface temperature,
air-sea fluxes, air-sea coupling, and upper ocean variability in
the PACS study region.
Project Goals:
Our specific analysis objectives are to
provide:
-
Accurate quantification of the air-sea
fluxes of heat, fresh water and momentum in the ITCZ/Cold
Tongue Complex (CTIC) region on times scales from hourly to
annual.
-
Description of the temporal evolution of
the upper ocean at two contrasting sites, cold tongue and ITCZ,
and quantification of the relative roles of ocean processes
and air-sea interaction in creating SST anomalies.
-
Analysis of a well-sampled meridional
section, 125°W, during a strong El Nino event.
Methodology:
Our analysis will examine the local interaction between the
atmosphere and ocean in the eastern tropical Pacific during the
1997-1998 warm event and during the onset of the ongoing cold
event using data from two air-sea interaction surface moorings and
three cruises in the region. This is the first time the complete
characterization of the air-sea exchange of heat, moisture and
momentum has been obtained for extended periods of time at remote
locations in the eastern tropical Pacific. Accurate fluxes of
momentum, heat, and freshwater will be determined using techniques
developed in TOGA COARE (Tropical Ocean-Global Atmosphere Coupled
Ocean Atmosphere Response Experiment). The fact that the 18 month
mooring record coincides perfectly with the one of the largest
ENSO warm events on record makes this data even more valuable.
Extensive collaborations with scientists from NCEP, ECMWF, NCAR,
NASA, SUNY, U. Miami, U. Washington and other institutions will
extend the scope of the analysis.
We will initially focus on the analysis of
upper ocean and air-sea flux variability and evolution in the two
regimes sampled by the moorings and contrast the air-sea
interaction at the two sites which at times spanned the meridional
gradients in SST associated with the cold tongue/ITCZ complex and
the onset of La Niña conditions. We will also explore the air-sea
fluxes in relation to convective variability and large-scale
atmospheric circulation during the 18 observing period.
Variability on time scales from instantaneous (60 sec) to diurnal
to seasonal to interannual would be explored. Associated with this
effort is the validation of the moored data by intercomparison of
redundant systems, evaluation of pre and post deployment
calibrations and ship-buoy intercomparison. This will assure that
we are working with a data set of the highest quality.
Results and Accomplishments:
We are only just starting analysis work and will update this
section as the project continues. We have just completed data
processing, quality control and documentation of all the moored
data during this project. A data report with the details of this
process is completed and will soon be available as a WHOI
Technical Report as will a CDROM containing the time series of
air-sea fluxes at the two sites. We have begun evaluation of
gridded products from ECMWF, NCEP, SSM/I and NSCAT.
Future Work:
We plan to analyze the ocean response and the processes that
govern the evolution of the upper ocean temperature, salinity and
velocity at each site and explore what extent is the local upper
ocean heat budget is dominated by surface heat fluxes, horizontal
advection, upwelling and entrainment. We seek to extend of our
understanding of the air-sea fluxes from the buoy sites to a wider
region in a cooperative effort with colleagues at NCEP, NASA,
ECMWF and Southhampton Oceanography Centre (UK). We will use the
highly accurate buoy fluxes to evaluate and contrast gridded
surface flux products derived from in situ, remotely sensed and
model fields. By completing the buoy-gridded product
intercomparison, we hope to identify systematic errors and improve
the fields for regional numerical studies. This would yield a firm
foundation and data set for testing tropical ocean models and
validating forecast model results. Clearly this is a region and
time when remote forcing led to dramatic changes in the
thermocline depth and horizontal advection of water masses. The
moored data record will allow us to quantify the role of a number
of physical processes at those two sites. Then, together with PACS
ocean modelers, we plan to explore in three dimensions the
physical processes that governed that large scale circulations and
hydrographic variability in the eastern tropical Pacific during
1997 and 1998.
Publications resulting from this research:
Anderson, S. P. and R. A. Weller, 1999: Air-sea interaction in
the eastern tropical Pacific: An experiment of the Pan American
Climate Study (PACS) during the 1997-1998 ENSO. Proceedings of the
23rd Conference on hurricanes and tropical meteorology.
10-15 January 1999, Dallas, TX. 143-144.
Way, B., W. Ostrom, R. Weller, J. Ware, R.
Trask, R. Cole, and J. Donovan, 1998: Pan American Climate Study
(PACS) Mooring Deployment Cruise Report, R/V Roger Revelle Cruise
Number 4, 9 April – 5 May 1997. WHOI Technical Report
WHOI-98-07, pp. 71.
Trask, R., R. Weller, W. Ostrom, B. Way, 1998:
Pan American Climate Study (PACS) Mooring Deployment Cruise
Report, R/V Thomas Thompson Cruise Number 73, 28 November to 26
December 1997. WHOI Technical Report WHOI-98-18, pp. 103.
Ostrom, W., B. Way, S. Anderson, B. Jones, E.
Key, G. Yuras, 1999: Pan American Climate Study (PACS) Mooring
Deployment Cruise Report, R/V Melville Cruise PACS03MV, 6
September to 30 September 1998. WHOI Technical Report WHOI-99-06,
pp. 74.
Anderson, S. P., K. Huang, N. Brink, M.
Baumgartner and R. Weller, 2000: Pan American Climate Studies Data
Report. WHOI Technical Report in press.
Contacts:
Principal Investigators:
Steven P. Anderson
sanderson@whoi.edu
Phone: (508) 289-2876
Fax: (508) 457-2163
Robert A. Weller
rweller@whoi.edu
Phone: (508) 289-2508
Fax: (508) 457-2163
Institution:
Woods Hole Oceanographic Institution
Woods Hole, Massachusetts 02543
Links:
http://www.whoi.edu
http://uop.whoi.edu
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